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| 1. Intoduction | 2. Site Characteristics | 3. The Chalk Aquifer | 4. Fracture Network Characteristics | |
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The fracture system was characterised using combined core logging and down-hole acoustic and optical televiewer imaging. Bedding-parallel fractures with a dominant ENE-WSW strike and dip of 2-29&Mac251; to the SSE and a subordinate bedding-parallel fracture set with E-W strike and N dip of 10-30&Mac251; High-angled fractures include sets with a ENE-WSW or E-W trend and NNW dip of 30 to 80&Mac251;, and sets with a NW-SE trend and NE dip of 35-75&Mac251; Mean fracture spacing for combined bedding-parallel and high-angled fractures is 0.23 m Fracture porosity is estimated as 1.1% and is similar to estimates from other studies |
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